Abstract

CH4–CO2 replacement is a carbon-negative, safer gas production technique to produce methane gas from natural gas hydrate reservoirs by injecting pure CO2 or other gas mixtures containing CO2. Laboratory-scale experiments show that this technique produces low methane volume and has a slow replacement rate due to the mass transfer barrier created due to impermeable CO2 hydrate layer formation, thus making the process commercially unattractive. This mass-transfer barrier can be reduced through pressure reduction techniques and chemical techniques; however, very few studies have focused on depressurization-assisted and chemical-assisted CH4–CO2 replacement to lower mass-transfer barriers and there are many unknowns. In this work, we qualitatively and quantitatively investigated the effect of the pressure reduction and presence of a hydrate promoter on mixed hydrate stability, CH4 recovery, and risk of water production during CH4–CO2 exchange. Exchange experiments were carried out using the 500 ppm sodium dodecyl sulfate (SDS) solution inside a high-pressure stirred reactor. Our results indicated that mixed hydrate stability and methane recovery depends on the degree of pressure reduction, type, and composition of injected gas. Final selection between CO2 and CO2 + N2 gas depends on the tradeoff between mixed hydrate stability pressure and methane recovery. Hydrate morphology studies suggest that production of water during the CH4–CO2 exchange is a stochastic phenomenon that is dependent on many parameters.

Highlights

  • Methane hydrates are considered to be a potential source of clean energy

  • Both qualitative and quantitative analyses are performed to study the effect of different degrees of immediate pressure reduction (IPR), type of gas injection on the stability of mixed gas hydrates, methane recovery efficiency, and risk of water production

  • Final selection of CO2 -rich gas during CH4 –CO2 replacement is based on a tradeoff between hydrate stability and methane-recovery efficiency

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Summary

Introduction

Methane hydrates are considered to be a potential source of clean energy. Gas hydrates are ice-like crystals, formed at low temperatures and in high-pressure conditions, having guest molecules of appropriate size and shape occupied inside water cages. A novel technique comprised of carbon dioxide (CO2 ) or CO2 + nitrogen (N2 ) gas mixture injection into methane hydrate was proposed to produce methane gas and sequestration of CO2 at the same time without disturbing the geo-mechanical stability [2]. This technology is still immature and there are many unknowns; for example, the reaction rate (kinetics), the stability of the mixed hydrates structures, structural changes, the recovery rate of methane, and the storage percentage of CO2 are currently under investigation

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